The first globally complete glacier inventory has been createdby Staff WritersDresden, Germany (SPX) May 08, 2014

Overall, glaciers cover an area of about 730,000 km2 and have a volume of about 170,000 km3.

Thanks to the efforts of an international group of scientists - one of them is Tobias Bolch from Technische Universitat Dresden, Germany - who have mapped all of the world's glaciers, glaciologists can now study with unprecedented accuracy the impacts of a changing climate on glaciers worldwide, and determine their total extent and volume on a glacier-by-glacier basis.

Overall, glaciers cover an area of about 730,000 km2 and have a volume of about 170,000 km3. The scientists found nearly 200,000 of them, but they say that this is the least important result of the mapping exercise as the number constantly changes due to disappearing small and fragmenting larger glaciers. More importantly, each glacier in the new inventory is represented by a computer-readable outline, making precise modelling of glacier-climate interactions much easier.

"This boost to the infrastructure means that people can now do research that they simply couldn't do properly before", said Graham Cogley of Trent University, one of the coordinators of the new Randolph Glacier Inventory (RGI), which is named after one of the group's meeting places in New Hampshire. The now published article is presenting the RGI and first statistical analysis of the global glacier distribution.

The main stimulus for completing the inventory was the recently-published Fifth Assessment of the Intergovernmental Panel on Climate Change (IPCC). Several studies that relied on earlier versions of the RGI were essential sources for that assessment.

"I don't think anyone could have made meaningful progress on projecting glacier changes if the Randolph inventory had not been available", said the University of Colorado's Tad Pfeffer, lead author of the study just published in the Journal of Glaciology. Like several of his co-authors, Pfeffer was also involved in the IPCC assessment.

The total extent of the glaciers in the RGI is about the size of Germany plus Switzerland and Poland. According to several studies, the corresponding total volume is between 35 and 47 cm of sea-level equivalent, i.e. sea level would rise by this amount when all glaciers would melt completely. This is less than most earlier estimates, and less than 1% of the amount stored in the Greenland and Antarctic Ice Sheets.

However, barring an unlikely catastrophic ice-sheet collapse the smaller glaciers are judged to be at much more immediate risk under the stress of climatic change as their ice is in general already at the melting point whereas the ice of the ice sheets has to be warmed up to zero degrees first. Glaciers currently contribute about 1/3 to the observed sea level rise, about the same as both ice sheets together (the remaining third is resulting from thermal expansion of ocean water).

"The rapid shrinkage of glaciers during the past 20 years is also well-recognizable in the Alps and other parts of the world" says Frank Paul from the University of Zurich, co-author of the study and also lead author of the first part of the IPCC report that was published in September last year.

"Here and in other parts of the world the diminishing glaciers also impact on regional to local scale hydrology, natural hazards, and livelihoods in otherwise dry mountain regions. Accurate knowledge of water reserves and their future evolution is thus key for local authorities for early implementation of mitigation measures" adds his colleague Tobias Bolch who is also researching at Technische Universitat Dresden, Germany.

Seeing the bedrock through the treesBerkeley CA (SPX) May 06, 2014
University of California, Berkeley, geologist William Dietrich pioneered the application of airborne LIDAR - light detection and ranging - to map mountainous terrain, stripping away the vegetation to see the underlying ground surface.
But that didn't take him deep enough. He still couldn't see what was under the surface: the depth of the soil, the underlying weathered rock and the deep bed ... read more

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